* I T IS known that the areal distribution of ice in the arctic seas varies greatly from year to year, and considerable work has been done in an effort to find an explanation for this phenomenon in order to d,evelop reliable methods good progress in this respect. As explained by Zubov (1948) the Rus...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.573.3319 2023-05-15T14:19:46+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.573.3319 http://pubs.aina.ucalgary.ca/arctic/Arctic9-4-249.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.573.3319 http://pubs.aina.ucalgary.ca/arctic/Arctic9-4-249.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic9-4-249.pdf text ftciteseerx 2016-01-08T12:38:02Z * I T IS known that the areal distribution of ice in the arctic seas varies greatly from year to year, and considerable work has been done in an effort to find an explanation for this phenomenon in order to d,evelop reliable methods good progress in this respect. As explained by Zubov (1948) the Russian method is based on the premise that “ice drifts along isobaric lines with a speed Text Arctic Arctic Unknown Arctic Zubov ENVELOPE(-65.883,-65.883,-65.700,-65.700) |
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* I T IS known that the areal distribution of ice in the arctic seas varies greatly from year to year, and considerable work has been done in an effort to find an explanation for this phenomenon in order to d,evelop reliable methods good progress in this respect. As explained by Zubov (1948) the Russian method is based on the premise that “ice drifts along isobaric lines with a speed |
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